A large-scale planetary wave whose restoring force is the variation of Coriolis parameter with latitude.Rossby waves are enormous, slow-moving meanders in the flow of planetary atmospheres and oceans. Unlike ordinary waves that need a surface or a density difference to travel, these waves arise because the Earth's rotation affects moving air and water differently at different latitudes. Their name is often applied to the wavy patterns seen in the jet stream, which can steer weather systems across continents.
The concept was identified by Carl-Gustaf Rossby in the late 1930s while he was studying the large-scale motions of the atmosphere.
Imagine a parcel of air displaced northward. Because the Earth's rotation is stronger (in terms of the Coriolis effect) at higher latitudes, the parcel experiences a restoring force that pushes it back south. But it overshoots, and the same effect pushes it north again, setting up a wave that propagates westward relative to the mean flow. In the ocean, the same physics creates slow, large-scale undulations of currents and sea surface height.
Rossby waves are key to medium-range weather forecasting, as their positions and movements influence the formation of high- and low-pressure systems.
Rossby waves in the ocean can take months to cross an ocean basin, yet they subtly influence sea surface temperatures and marine ecosystems.








